The Roles of CO₂ and Orbital Forcing in Driving Southern Hemispheric Temperature Variations during the Last 21 000 Yr

Transient climate model simulations covering the last 21 000 yr reveal that orbitally driven insolation changes in the Southern Hemisphere, combined with a rise in atmospheric pCO₂, were sufficient to jumpstart the deglacial warming around Antarctica without direct Northern Hemispheric triggers. Ana...

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Published inJournal of climate Vol. 22; no. 7; pp. 1626 - 1640
Main Authors Timmermann, Axel, Timm, Oliver, Stott, Lowell, Menviel, Laurie
Format Journal Article
LanguageEnglish
Published Boston, MA American Meteorological Society 01.04.2009
Subjects
Albedo
Antarctic regions
Atmospherics
Carbon dioxide
Carbon dioxide concentration
Climate change
Climate models
Earth sciences
Earth, ocean, space
Exact sciences and technology
Gases
Greenhouse effect
Greenhouse gases
Heat
Hydrology
Ice
Ice cores
Ice sheets
Insolation
Isotopes
Marine and continental quaternary
Meteorology
Ozone
Paleoclimatology
Sea ice
Seasonal variations
Seasons
Simulation
Simulations
Southern Hemisphere
Summer
Surficial geology
Temperature
Temperature variations
Terminations
Southern Hemisphere
Antarctica
Southern Ocean
Insolation
Carbon dioxide
Atmosphere cryosphere interaction
digital simulation
upper Quaternary
greenhouse gas
feedback
Wurm
sea ice
Forcing
Cenozoic
Triggering
albedo
climate change
Southern Hemisphere
climate variations
Quaternary
climate warming
Orbital element
Climate models
deglaciation
Dynamical climatology
upper Pleistocene
Phanerozoic
Holocene
Pleistocene
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Abstract Transient climate model simulations covering the last 21 000 yr reveal that orbitally driven insolation changes in the Southern Hemisphere, combined with a rise in atmospheric pCO₂, were sufficient to jumpstart the deglacial warming around Antarctica without direct Northern Hemispheric triggers. Analyses of sensitivity experiments forced with only one external forcing component (greenhouse gases, ice-sheet forcing, or orbital forcing) demonstrate that austral spring insolation changes triggered an early retreat of Southern Ocean sea ice starting around 19–18 ka BP. The associated sea ice–albedo feedback and the subsequent increase of atmospheric CO₂ concentrations helped to further accelerate the deglacial warming in the Southern Hemisphere. Implications for the interpretation of Southern Hemispheric paleoproxy records are discussed.
AbstractList Transient climate model simulations covering the last 21 000 yr reveal that orbitally driven insolation changes in the Southern Hemisphere, combined with a rise in atmospheric pCO₂, were sufficient to jumpstart the deglacial warming around Antarctica without direct Northern Hemispheric triggers. Analyses of sensitivity experiments forced with only one external forcing component (greenhouse gases, ice-sheet forcing, or orbital forcing) demonstrate that austral spring insolation changes triggered an early retreat of Southern Ocean sea ice starting around 19–18 ka BP. The associated sea ice–albedo feedback and the subsequent increase of atmospheric CO₂ concentrations helped to further accelerate the deglacial warming in the Southern Hemisphere. Implications for the interpretation of Southern Hemispheric paleoproxy records are discussed.
Transient climate model simulations covering the last 21 000 yr reveal that orbitally driven insolation changes in the Southern Hemisphere, combined with a rise in atmospheric pCO^sub 2^, were sufficient to jump-start the deglacial warming around Antarctica without direct Northern Hemispheric triggers. Analyses of sensitivity experiments forced with only one external forcing component (greenhouse gases, ice-sheet forcing, or orbital forcing) demonstrate that austral spring insolation changes triggered an early retreat of Southern Ocean sea ice starting around 19-18 ka BP. The associated sea ice-albedo feedback and the subsequent increase of atmospheric CO2 concentrations helped to further accelerate the deglacial warming in the Southern Hemisphere. Implications for the interpretation of Southern Hemispheric paleoproxy records are discussed. [PUBLICATION ABSTRACT]
Transient climate model simulations covering the last 21 000 yr reveal that orbitally driven insolation changes in the Southern Hemisphere, combined with a rise in atmospheric pCO2, were sufficient to jump-start the deglacial warming around Antarctica without direct Northern Hemispheric triggers. Analyses of sensitivity experiments forced with only one external forcing component (greenhouse gases, ice-sheet forcing, or orbital forcing) demonstrate that austral spring insolation changes triggered an early retreat of Southern Ocean sea ice starting around 19–18 ka BP. The associated sea ice–albedo feedback and the subsequent increase of atmospheric CO2 concentrations helped to further accelerate the deglacial warming in the Southern Hemisphere. Implications for the interpretation of Southern Hemispheric paleoproxy records are discussed.
Abstract Transient climate model simulations covering the last 21 000 yr reveal that orbitally driven insolation changes in the Southern Hemisphere, combined with a rise in atmospheric pCO2, were sufficient to jump-start the deglacial warming around Antarctica without direct Northern Hemispheric triggers. Analyses of sensitivity experiments forced with only one external forcing component (greenhouse gases, ice-sheet forcing, or orbital forcing) demonstrate that austral spring insolation changes triggered an early retreat of Southern Ocean sea ice starting around 19–18 ka BP. The associated sea ice–albedo feedback and the subsequent increase of atmospheric CO2 concentrations helped to further accelerate the deglacial warming in the Southern Hemisphere. Implications for the interpretation of Southern Hemispheric paleoproxy records are discussed.
Author Timmermann, Axel
Timm, Oliver
Stott, Lowell
Menviel, Laurie
Author_xml – sequence: 1
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  surname: Timmermann
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– sequence: 4
  givenname: Laurie
  surname: Menviel
  fullname: Menviel, Laurie
  organization: Department of Oceanography, SOEST, University of Hawaii at Manoa, Honolulu, Hawaii
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Issue 7
Keywords Insolation
Carbon dioxide
Atmosphere cryosphere interaction
digital simulation
upper Quaternary
greenhouse gas
feedback
Wurm
sea ice
Forcing
Cenozoic
Triggering
albedo
climate change
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Climate models
deglaciation
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upper Pleistocene
Phanerozoic
Holocene
Pleistocene
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  year: 1996
  ident: 2020061414290407100_i1520-0442-22-7-1626-Brook1
  article-title: Rapid variations in atmospheric methane concentration during the past 110,000 years.
  publication-title: Science
  doi: 10.1126/science.273.5278.1087
  contributor:
    fullname: Brook
SSID ssj0012600
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Snippet Transient climate model simulations covering the last 21 000 yr reveal that orbitally driven insolation changes in the Southern Hemisphere, combined with a...
Abstract Transient climate model simulations covering the last 21 000 yr reveal that orbitally driven insolation changes in the Southern Hemisphere, combined...
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SubjectTerms Albedo
Antarctic regions
Atmospherics
Carbon dioxide
Carbon dioxide concentration
Climate change
Climate models
Earth sciences
Earth, ocean, space
Exact sciences and technology
Gases
Greenhouse effect
Greenhouse gases
Heat
Hydrology
Ice
Ice cores
Ice sheets
Insolation
Isotopes
Marine and continental quaternary
Meteorology
Ozone
Paleoclimatology
Sea ice
Seasonal variations
Seasons
Simulation
Simulations
Southern Hemisphere
Summer
Surficial geology
Temperature
Temperature variations
Terminations
Title The Roles of CO₂ and Orbital Forcing in Driving Southern Hemispheric Temperature Variations during the Last 21 000 Yr
URI https://www.jstor.org/stable/26260485
https://www.proquest.com/docview/222895530/abstract/
https://www.proquest.com/docview/2818802066/abstract/
Volume 22
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